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Nimmitabel, New South Wales
Nimmitabel is a small town in the Monaro region in southeast New South Wales, Australia, in the Snowy Monaro Regional Council local government area. At the , Nimmitabel had a population of 320. Etymology Nimmitabel means "the place where many waters start or divide" in the local Aboriginal language. Many various spellings were adopted for the town, including: Nimmytabell (1837), Nimmitabool (1841), Nimmittybel (1844), Nimmitabel(1845), Nimmitybelle, Nimithybale, Nymytable (all in 1848), Nimmitabil(1851), Nimitabille and Nimithy Bell(1856), Nimaty-Bell(1857), Nimmitabel(1858) Geography The town is south of Cooma and west of Bega. Nimmitabel is on a stretch of highway shared between the Snowy Mountains Highway (HWY B72) and the Monaro Highway (HWY B23). It is on the southern end of the Great Dividing Range, at the west of the Monaro Range, and lies west of the Wadbilliga National Park. The area around Nimmitabel has the only true chernozem soil in Australia, a very rich, f ...
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Electoral District Of Monaro
Monaro, also known as Maneroo (1856–1858), Monara (1858–1879) and Manaro (1894–1904) is an New South Wales Legislative Assembly electoral districts, electoral district of the New South Wales Legislative Assembly, Legislative Assembly in the Australian state of New South Wales. It is currently represented by Nichole Overall of the National Party of Australia – NSW, National Party. Monaro is a regional district in the south of the state. It encompasses the Queanbeyan-Palerang Regional Council and Snowy Monaro Regional Council. Its significant population centres include Queanbeyan, New South Wales, Queanbeyan, Bungendore, New South Wales, Bungendore, Braidwood, New South Wales, Braidwood, Cooma, New South Wales, Cooma, Bombala, New South Wales, Bombala, Captains Flat, New South Wales, Captains Flat, Nimmitabel, New South Wales, Nimmitabel, Delegate, New South Wales, Delegate, Bredbo, New South Wales, Bredbo, Michelago, New South Wales, Michelago, Berridale, New South Wales, ...
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Wadbilliga National Park
Wadbilliga National Park is a national park that is located in high country spanning the Monaro and South Coast regions of south-eastern New South Wales, Australia. Location and features Wadbilliga National Park is located southwest of Sydney via Cobargo, and south east of Canberra. The nearest towns are Narooma and Cobargo in the east, and Cooma on the plateau in the west. Wadbilliga is a wilderness area, and much of its protected area is in a near pristine state. Featuring rugged gorges and gullies. Suited to overnight camping and wilderness walking (only for the most experienced and well prepared). Areas of interest include the Tuross Falls, the Tuross River Gorge and Brogo Wilderness Area. The Wadbilliga Track is a scenic four wheel drive road which travels up the escarpment from east to west. Wadbilliga is in a remote part of Australia, and has had little influence from mankind in the history of European settlement. In recent decades, it has become protected, and has in ...
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The Sundowners (1960 Film)
''The Sundowners'' is a 1960 Technicolor comedy drama film that tells the story of a 1920s Australian outback family torn between the father's desires to continue his nomadic sheep-herding ways and the wife's and son's desire to settle down in one place. ''The Sundowners'' was produced and directed by Fred Zinnemann, adapted by Isobel Lennart from Jon Cleary's 1952 novel of the same name, and starring Deborah Kerr, Robert Mitchum and Peter Ustinov, with a supporting cast including Glynis Johns, Mervyn Johns, Dina Merrill, Michael Anderson Jr. and Chips Rafferty. The screenplay was adapted by Isobel Lennart from Jon Cleary's 1952 novel of the same name; it was produced and directed by Fred Zinnemann. In 2019, FilmInk cited it among “50 meat pie Westerns”. At the 33rd Academy Awards, it was in the running for Best Picture, while Kerr was nominated for Best Actress in a Leading Role, Johns for Best Actress in a Supporting Role, Zinnemann for Best Director, and Lennart ...
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Railway
Rail transport (also known as train transport) is a means of transport that transfers passengers and goods on wheeled vehicles running on rails, which are incorporated in tracks. In contrast to road transport, where the vehicles run on a prepared flat surface, rail vehicles (rolling stock) are directionally guided by the tracks on which they run. Tracks usually consist of steel rails, installed on sleepers (ties) set in ballast, on which the rolling stock, usually fitted with metal wheels, moves. Other variations are also possible, such as "slab track", in which the rails are fastened to a concrete foundation resting on a prepared subsurface. Rolling stock in a rail transport system generally encounters lower frictional resistance than rubber-tyred road vehicles, so passenger and freight cars (carriages and wagons) can be coupled into longer trains. The operation is carried out by a railway company, providing transport between train stations or freight customer facilit ...
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Courthouse
A courthouse or court house is a building that is home to a local court of law and often the regional county government as well, although this is not the case in some larger cities. The term is common in North America. In most other English-speaking countries, buildings which house courts of law are simply called "courts" or "court buildings". In most of continental Europe and former non-English-speaking European colonies, the equivalent term is a palace of justice ( French: ''palais de justice'', Italian: ''palazzo di giustizia'', Portuguese: ''palácio da justiça''). United States In most counties in the United States, the local trial courts conduct their business in a centrally located courthouse. The courthouse may also house other county government offices, or the courthouse may consist of a designated part of a wider county government building or complex. The courthouse is usually located in the county seat, although large metropolitan counties may have satellite or ...
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Post Office
A post office is a public facility and a retailer that provides mail services, such as accepting letters and parcels, providing post office boxes, and selling postage stamps, packaging, and stationery. Post offices may offer additional services, which vary by country. These include providing and accepting government forms (such as passport applications), and processing government services and fees (such as road tax, postal savings, or bank fees). The chief administrator of a post office is called a postmaster. Before the advent of postal codes and the post office, postal systems would route items to a specific post office for receipt or delivery. During the 19th century in the United States, this often led to smaller communities being renamed after their post offices, particularly after the Post Office Department began to require that post office names not be duplicated within a state. Name The term "post-office" has been in use since the 1650s, shortly after the legali ...
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Public House
A pub (short for public house) is a kind of drinking establishment which is licensed to serve alcoholic drinks for consumption on the premises. The term ''public house'' first appeared in the United Kingdom in late 17th century, and was used to differentiate private houses from those which were, quite literally, open to the public as "alehouses", "taverns" and "inns". By Georgian times, the term had become common parlance, although taverns, as a distinct establishment, had largely ceased to exist by the beginning of the 19th century. Today, there is no strict definition, but CAMRA states a pub has four characteristics:GLA Economics, Closing time: London's public houses, 2017 # is open to the public without membership or residency # serves draught beer or cider without requiring food be consumed # has at least one indoor area not laid out for meals # allows drinks to be bought at a bar (i.e., not only table service) The history of pubs can be traced to Roman taverns in B ...
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Church (building)
A church, church building or church house is a building used for Christian worship services and other Christian religious activities. The earliest identified Christian church is a house church founded between 233 and 256. From the 11th through the 14th centuries, there was a wave of church construction in Western Europe. Sometimes, the word ''church'' is used by analogy for the buildings of other religions. ''Church'' is also used to describe the Christian religious community as a whole, or a body or an assembly of Christian believers around the world. In traditional Christian architecture, the plan view of a church often forms a Christian cross; the center aisle and seating representing the vertical beam with the Church architecture#Characteristics of the early Christian church building, bema and altar forming the horizontal. Towers or domes may inspire contemplation of the heavens. Modern churches have a variety of architectural styles and layouts. Some buildings designe ...
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Snowfalls
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is col ...
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Frost
Frost is a thin layer of ice on a solid surface, which forms from water vapor in an above-freezing atmosphere coming in contact with a solid surface whose temperature is below freezing, and resulting in a phase change from water vapor (a gas) to ice (a solid) as the water vapor reaches the freezing point. In temperate climates, it most commonly appears on surfaces near the ground as fragile white crystals; in cold climates, it occurs in a greater variety of forms. The propagation of crystal formation occurs by the process of nucleation. The ice crystals of frost form as the result of fractal process development. The depth of frost crystals varies depending on the amount of time they have been accumulating, and the concentration of the water vapor (humidity). Frost crystals may be invisible (black), clear (translucent), or white; if a mass of frost crystals scatters light in all directions, the coating of frost appears white. Types of frost include crystalline frost (hoar fro ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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Maritime Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. ...
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